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The Carboniferous Evolution of Nova Scotia

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The Carboniferous Evolution of Nova Scotia Downloaded from http://sp.lyellcollection.org/ by guest on September 27, 2021 The Carboniferous evolution of Nova Scotia J. H. CALDER Nova Scotia Department of Natural Resources, PO Box 698, Halifax, Nova Scotia, Canada B3J 2T9 Abstract: Nova Scotia during the Carboniferous lay at the heart of palaeoequatorial Euramerica in a broadly intermontane palaeoequatorial setting, the Maritimes-West-European province; to the west rose the orographic barrier imposed by the Appalachian Mountains, and to the south and east the Mauritanide-Hercynide belt. The geological affinity of Nova Scotia to Europe, reflected in elements of the Carboniferous flora and fauna, was mirrored in the evolution of geological thought even before the epochal visits of Sir Charles Lyell. The Maritimes Basin of eastern Canada, born of the Acadian-Caledonian orogeny that witnessed the suture of Iapetus in the Devonian, and shaped thereafter by the inexorable closing of Gondwana and Laurasia, comprises a near complete stratal sequence as great as 12 km thick which spans the Middle Devonian to the Lower Permian. Across the southern Maritimes Basin, in northern Nova Scotia, deep depocentres developed en echelon adjacent to a transform platelet boundary between terranes of Avalon and Gondwanan affinity. The subsequent history of the basins can be summarized as distension and rifting attended by bimodal volcanism waning through the Dinantian, with marked transpression in the Namurian and subsequent persistence of transcurrent movement linking Variscan deformation with Mauritainide-Appalachian convergence and Alleghenian thrusting. This Mid- Carboniferous event is pivotal in the Carboniferous evolution of Nova Scotia. Rapid subsidence adjacent to transcurrent faults in the early Westphalian was succeeded by thermal sag in the later Westphalian and ultimately by basin inversion and unroofing after the early Permian as equatorial Pangaea finally assembled and subsequently rifted again in the Triassic. The component Carboniferous basins have provided Nova Scotia with its most important source of mineral and energy resources for three centuries. Their combined basin-fill sequence preserves an exceptional record of the Carboniferous terrestrial ecosystems of palaeoequatorial Euramerica, interrupted only in the mid-late Visran by the widespread marine deposits of the hypersaline Windsor gulf; their fossil record is here compiled for the first time. Stratal cycles in the marine Windsor, schizohaline Mabou and coastal plain to piedmont coal measures 'cyclothems' record Nova Scotia's palaeogeographic evolution and progressively waning marine influence. The semiarid palaeoclimate of the late Dinantian grew abruptly more seasonally humid after the Namurian and gradually recurred by the Lower Permian, mimicking a general Euramerican trend. Generally more continental and seasonal conditions prevailed than in contemporary basins to the west of the Appalachians and, until the mid-Westphalian, to the east in Europe. Palaeogeographic, paleoflow and faunal trends point to the existence of a Mid- Euramerican Sea between the Maritimes and Europe which persisted through the Carboniferous. The faunal record suggests that cryptic expressions of its most landward transgressions can be recognized within the predominantly continental strata of Nova Scotia. I never travelled in any country where my geological affinity of Nova Scotia to Europe, scientific pursuits seemed to be better under- recorded in elements of the Carboniferous flora and stood, or were more zealously forwarded, than in fauna, reflects its palaeogeographic position during Nova Scotia... (Lyell, 1845, pp. 229-230) the Carboniferous at the heart of palaeoequatorial Euramerica, in proximity to western Europe. If not The geological evolution of Nova Scotia during a Euramerican Rosetta Stone, Nova Scotia and the the Carboniferous and the evolution of geological Maritimes certainly from the keystone in the bridge thought about the Carboniferous strata in Nova to understanding the Carboniferous evolution of Scotia both record a strong affinity to western North America and Europe (Lyell 1843a, 1845; Europe. During the nineteenth century, the splendid Dawson 1888; Belt 1968a, 1969; Carroll et al. coastal exposures of Carboniferous strata (Fig. 1) 1972; Bless et al. 1987; Allen & Dineley 1988; were proving grounds for the geological principles Leeder 1988a; McKerrow 1988; Calder & Gibling and philosophy of Sir Charles Lyell, especially as 1994, among many others). they pertained to the Carboniferous Period. The In this paper, the Carboniferous evolution of CALDER, J. H. 1998. The Carboniferous evolution of Nova Scotia. In: BLUNDELL,D. J. & Scor-r, A. C. (eds) 261 Lyell: the Past is the Key to the Present. Geological Society, London, Special Publications, 143, 261-302. Downloaded from http://sp.lyellcollection.org/ by guest on September 27, 2021 262 J.H. CALDER Fig. 1. The Carboniferous section at Joggins, of which Lyell, in a discussion of coal measures in his The Student's Elements of Geology (1871), wrote, "But the finest example in the world of a natural exposure in a continuous section ten miles long, occurs in the sea-cliffs bordering a branch of the Bay of Fundy in Nova Scotia." From a nineteenth- century wood block engraving in Dawson's Acadian Geology. Nova Scotia is considered by linking its tectonic northeasterly trending intermontane basins, once history, basin fill sequence, fossil record and variously interconnected and now, as then, defined palaeoclimate with those of Carboniferous by intervening massifs of the Avalon, Grenville and Euramerica to the west in North America and to the Meguma terranes. The basin was born of the east in Europe. The aim of the paper is not only to Devonian (Emsian) Acadian orogeny (Poole 1967), review, but also to relate the records of disparate contemporary of the latest stage of the Caledonian geological disciplines and to consider, from the orogeny, both of which record final closure of the author's perspective, implications that emerge for Iapetus Ocean (McKerrow 1988). The Carbon- long established views of the Carboniferous history iferous evolution of the Maritimes Basin bears of Nova Scotia. A detailed treatment of all witness to the nativity of Pangaea as Gondwana and stratigraphic units of the Maritimes Basin in Nova numerous platelets of suspect terrane collided with Scotia is neither intended nor possible in a paper of Laurasia and the Old Red Continent, manifested in this length. The references in this paper, as well as the Hercynian and Alleghenian orogenies (Schenk the overview of Gibling (1995, in van de Poll et al. 1981; Rast 1988). The evolution of the Maritimes 1995) and the Lexicon of Williams et al. (1985) will Basin during the late Devonian and Dinantian provide the reader with access to further details of records extension (McCutcheon & Robinson 1987; the Carboniferous stratigraphy and geology of Bradley 1982; Hamblin & Rust 1989) most Nova Scotia. pronounced between the Lubec-Bellisle, Cobequid and Hollow faults, an area that has been termed the Maritimes Rift (Belt 1969; van de Poll et al. 1995). Geological setting: the Maritimes Basin in This was suceeded in the Silesian by transpression and transtension in a renewed orogenic phase (Plint Euramerica & van de Poll 1984; Nance 1987; Waldron et al. The Carboniferous strata of Nova Scotia record 1989; Yeo & Ruixiang 1987) and broadly across the most of the history of the larger, Late Palaeozoic basin by thermal sag (Bradley 1982) and ultimately Maritimes Basin (Williams 1974) of New in the Permo-Triassic, by inversion (Ryan & Brunswick, Nova Scotia, Prince Edward Island and Zentilli 1993). Newfoundland (Fig. 2). The Late Palaeozoic strata Nova Scotia and the Maritimes Basin in the of the Maritimes Basin span the Middle Devonian Carboniferous lay within palaeoequatorial (Dawson 1862; McGregor 1977; Forbes et al. Euramerica, drifting northwards from a palaeo- 1979) through early Permian (Dawson 1845, 1891; latitude of 12 degrees south to cross the equator by Barss et al. 1963) with remarkably few gaps. The the beginning of the Permian (Scotese & Maritimes Basin is a complex of predominantly McKerrow 1990). Generally considered a northern Downloaded from http://sp.lyellcollection.org/ by guest on September 27, 2021 CARBONIFEROUS EVOLUTION OF NOVA SCOTIA 263 /j New Brunswick /~--~/ " .~ /(.,'. ~..,,'# .... - " i . ~ / i/~i/m e s 4e~ ~ B a s i n ', il - [ r ,, ,..~. / ~,/ w.~ /1%~:) , < ~ ,0~ ~" , ~ "---,---~--2_~ .... ( + " 9 ~Im "~ o~ ~, ~ P.E.I.< ~ ', .- + '' '" '" " ~a~ ~'f--'.: ' Basin ! 8,~':r _~. ~_~ Mahone Bay / ~ y.5 Outli~ I ,V Fig. 2. Areas underlain by Middle Devonian - Permo-Carboniferous strata of the southern Maritimes Basin in Nova Scotia, and neighbouring provinces, with component depositional basins and intrabasinal massifs; modified after Gibling et al. (1992) and Gibling (1995). part of the Appalachian orogenic belt, the The evolution of geological thought on the Maritimes Basin lay situated at the palaeosouth- Carboniferous of Nova Scotia eastern margin of the Appalachians in a palaeo- geographic region distinct from the Appalachian The first comprehensive account of the Carbon- Basin to the west. The mountain range posed an iferous geology and mineral resources of Nova orographic climate barrier, drainage divide and Scotia is that of Richard Brown (Fig. 3) in 1829, phytogeographic barrier to biotic exchange although this contribution in the past, if not between these two areas. No such land barrier
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